Migration of the subtropical front as a modulator of glacial climate.
Ice cores extracted from the Antarctic ice sheet suggest that glacial conditions, and the relationship between isotopically derived temperatures and atmospheric PCO(2) have been constant over the last 800,000 years of the Late Pleistocene epoch. But independent lines of evidence, such as the extent...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2009
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